The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization
International audience Uranium mineralization in the Kiggavik area, on the eastern border of the Thelon basin (Nunavut, Canada), hosts significant uranium resources within the basement and its understanding is critical to comprehending the genesis of unconformity-related deposits' structural co...
Published in: | Ore Geology Reviews |
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Main Authors: | , , , , , , |
Other Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2018
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Online Access: | https://hal.sorbonne-universite.fr/hal-01675254 https://hal.sorbonne-universite.fr/hal-01675254/document https://hal.sorbonne-universite.fr/hal-01675254/file/Grare%20et%20al.%20%282017%29%20The%20Contact%20prospect%20-%20Vers%20comb%20manuscr3.pdf https://doi.org/10.1016/j.oregeorev.2017.12.015 |
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Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
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ftccsdartic |
language |
English |
topic |
Uranium deposit alteration structural control fracture Thelon Basin Kiggavik [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
spellingShingle |
Uranium deposit alteration structural control fracture Thelon Basin Kiggavik [SDU.STU]Sciences of the Universe [physics]/Earth Sciences Grare, Alexis Benedicto, Antonio Lacombe, Olivier Trave, Anna Ledru, Patrick Blain, Mario Robbins, John The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization |
topic_facet |
Uranium deposit alteration structural control fracture Thelon Basin Kiggavik [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience Uranium mineralization in the Kiggavik area, on the eastern border of the Thelon basin (Nunavut, Canada), hosts significant uranium resources within the basement and its understanding is critical to comprehending the genesis of unconformity-related deposits' structural controls and therefore exploration of these types of deposits in this prospective district. This article deciphers the complex multiphase fracture network associated with uranium mineralization of the most recently discovered, basement-hosted prospect in the Kiggavik area, named Contact. The Contact prospect is located along the Andrew Lake Fault (ALF), a major NE-SW fault corridor in the area. This study combines field work, drillcore logging, sampling, and macro-to micro-petro-structural analyses. Key results from this study highlight that the NE-trending ALF, along with the ENE-trending Thelon (TF) and Judge Sissons (JSF) faults, formed early during intracratonic rifting and deposition of the Baker Lake and Wharton groups (ca. 1850–1750 Ma) in response to the Thelon and Trans-Hudsonian orogeny. The ALF was affected by a strong silicification-brecciation event that likely developed at ca. 1750 Ma, and partitioned later deformation and fluid circulation. In the Contact prospect, the ALF was reactivated multiple times and mineralized in three stages with distinctive secondary fracture patterns, alteration, and mineralization types. Ten fracture stages have been identified at the Contact prospect, f1 to f10. The first stage of mineralization, coeval with f5, is related to fluids of unconstrained origin that circulated through E-W faults in the area that locally reactivated quartz veins of the brecciation event at the intersection with the ALF. Mineralization at this stage is polymetallic and associated with weak clay alteration. The second stage of uranium mineralization occurred coeval with transtensional reactivation of the NE-SW trending ALF (f6c) and in relation to circulation of oxidizing basinal brines within the ... |
author2 |
Déformations, sismotectonique, imagerie, relief (DéSIR) Institut des Sciences de la Terre de Paris (iSTeP) Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS) |
format |
Article in Journal/Newspaper |
author |
Grare, Alexis Benedicto, Antonio Lacombe, Olivier Trave, Anna Ledru, Patrick Blain, Mario Robbins, John |
author_facet |
Grare, Alexis Benedicto, Antonio Lacombe, Olivier Trave, Anna Ledru, Patrick Blain, Mario Robbins, John |
author_sort |
Grare, Alexis |
title |
The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization |
title_short |
The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization |
title_full |
The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization |
title_fullStr |
The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization |
title_full_unstemmed |
The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization |
title_sort |
contact uranium prospect, kiggavik project, nunavut (canada): tectonic history, structural constraints and timing of mineralization |
publisher |
HAL CCSD |
publishDate |
2018 |
url |
https://hal.sorbonne-universite.fr/hal-01675254 https://hal.sorbonne-universite.fr/hal-01675254/document https://hal.sorbonne-universite.fr/hal-01675254/file/Grare%20et%20al.%20%282017%29%20The%20Contact%20prospect%20-%20Vers%20comb%20manuscr3.pdf https://doi.org/10.1016/j.oregeorev.2017.12.015 |
long_lat |
ENVELOPE(-86.117,-86.117,-77.917,-77.917) ENVELOPE(-54.765,-54.765,49.667,49.667) ENVELOPE(157.817,157.817,-81.050,-81.050) |
geographic |
Alf Canada Nunavut The Baker Wharton |
geographic_facet |
Alf Canada Nunavut The Baker Wharton |
genre |
Baker Lake Nunavut |
genre_facet |
Baker Lake Nunavut |
op_source |
ISSN: 0169-1368 Ore Geology Reviews https://hal.sorbonne-universite.fr/hal-01675254 Ore Geology Reviews, Elsevier, 2018, 93, pp.141 - 167. ⟨10.1016/j.oregeorev.2017.12.015⟩ |
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info:eu-repo/semantics/altIdentifier/doi/10.1016/j.oregeorev.2017.12.015 hal-01675254 https://hal.sorbonne-universite.fr/hal-01675254 https://hal.sorbonne-universite.fr/hal-01675254/document https://hal.sorbonne-universite.fr/hal-01675254/file/Grare%20et%20al.%20%282017%29%20The%20Contact%20prospect%20-%20Vers%20comb%20manuscr3.pdf doi:10.1016/j.oregeorev.2017.12.015 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1016/j.oregeorev.2017.12.015 |
container_title |
Ore Geology Reviews |
container_volume |
93 |
container_start_page |
141 |
op_container_end_page |
167 |
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1766366242717827072 |
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ftccsdartic:oai:HAL:hal-01675254v1 2023-05-15T15:35:54+02:00 The Contact uranium prospect, Kiggavik project, Nunavut (Canada): Tectonic history, structural constraints and timing of mineralization Grare, Alexis Benedicto, Antonio Lacombe, Olivier Trave, Anna Ledru, Patrick Blain, Mario Robbins, John Déformations, sismotectonique, imagerie, relief (DéSIR) Institut des Sciences de la Terre de Paris (iSTeP) Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS) 2018-02 https://hal.sorbonne-universite.fr/hal-01675254 https://hal.sorbonne-universite.fr/hal-01675254/document https://hal.sorbonne-universite.fr/hal-01675254/file/Grare%20et%20al.%20%282017%29%20The%20Contact%20prospect%20-%20Vers%20comb%20manuscr3.pdf https://doi.org/10.1016/j.oregeorev.2017.12.015 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.oregeorev.2017.12.015 hal-01675254 https://hal.sorbonne-universite.fr/hal-01675254 https://hal.sorbonne-universite.fr/hal-01675254/document https://hal.sorbonne-universite.fr/hal-01675254/file/Grare%20et%20al.%20%282017%29%20The%20Contact%20prospect%20-%20Vers%20comb%20manuscr3.pdf doi:10.1016/j.oregeorev.2017.12.015 info:eu-repo/semantics/OpenAccess ISSN: 0169-1368 Ore Geology Reviews https://hal.sorbonne-universite.fr/hal-01675254 Ore Geology Reviews, Elsevier, 2018, 93, pp.141 - 167. ⟨10.1016/j.oregeorev.2017.12.015⟩ Uranium deposit alteration structural control fracture Thelon Basin Kiggavik [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2018 ftccsdartic https://doi.org/10.1016/j.oregeorev.2017.12.015 2021-12-05T02:44:15Z International audience Uranium mineralization in the Kiggavik area, on the eastern border of the Thelon basin (Nunavut, Canada), hosts significant uranium resources within the basement and its understanding is critical to comprehending the genesis of unconformity-related deposits' structural controls and therefore exploration of these types of deposits in this prospective district. This article deciphers the complex multiphase fracture network associated with uranium mineralization of the most recently discovered, basement-hosted prospect in the Kiggavik area, named Contact. The Contact prospect is located along the Andrew Lake Fault (ALF), a major NE-SW fault corridor in the area. This study combines field work, drillcore logging, sampling, and macro-to micro-petro-structural analyses. Key results from this study highlight that the NE-trending ALF, along with the ENE-trending Thelon (TF) and Judge Sissons (JSF) faults, formed early during intracratonic rifting and deposition of the Baker Lake and Wharton groups (ca. 1850–1750 Ma) in response to the Thelon and Trans-Hudsonian orogeny. The ALF was affected by a strong silicification-brecciation event that likely developed at ca. 1750 Ma, and partitioned later deformation and fluid circulation. In the Contact prospect, the ALF was reactivated multiple times and mineralized in three stages with distinctive secondary fracture patterns, alteration, and mineralization types. Ten fracture stages have been identified at the Contact prospect, f1 to f10. The first stage of mineralization, coeval with f5, is related to fluids of unconstrained origin that circulated through E-W faults in the area that locally reactivated quartz veins of the brecciation event at the intersection with the ALF. Mineralization at this stage is polymetallic and associated with weak clay alteration. The second stage of uranium mineralization occurred coeval with transtensional reactivation of the NE-SW trending ALF (f6c) and in relation to circulation of oxidizing basinal brines within the ... Article in Journal/Newspaper Baker Lake Nunavut Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Alf ENVELOPE(-86.117,-86.117,-77.917,-77.917) Canada Nunavut The Baker ENVELOPE(-54.765,-54.765,49.667,49.667) Wharton ENVELOPE(157.817,157.817,-81.050,-81.050) Ore Geology Reviews 93 141 167 |